Why this matters
Forcan Ridge is a sea cliff composed primarily of basalt, formed during the Paleogene period through volcanic activity associated with the North Atlantic Igneous Province. It is notable for its columnar jointing, a result of the rapid cooling of lava flows, and its contribution to the dramatic coastal landscape of the Scottish Highlands.
What is recorded here
Forcan Ridge is shown as a cliff on the public map of Highland. The saved point is the map point or the centre of its mapped shape.
The public map does not by itself grant access. Check current paths, opening conditions and ownership before entering.